lateralEarthPressures: Lateral Earth Pressures

Description Usage Arguments Details Value Author(s) References See Also Examples

Description

These functions are used to calculate lateral earth pressure coefficients using different methods.

Usage

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K(sigmax, sigmaz)
Ko(phi, OCR = 1)
Ka(phi, beta = 0)
Kp(phi, beta = 0)

Arguments

sigmax

horizontal effective stress

sigmaz

vertical effective stress

phi

effective friction angle (deg)

OCR

overconsolidation ratio; default = 1

beta

angle of backfill (deg); default = 0

Details

These functions either compute the lateral earth pressure coefficient from provided stresses (K), common empirical correlations (Ka), or basic lateral earth pressure theories (Kp).

Value

Author(s)

James Kaklamanos <kaklamanosj@merrimack.edu> and Kyle Elmy <ElmyK@merrimack.edu>

References

Jaky, J. (1944). "The Coefficient of Earth Pressure at Rest", Journal for the Society of Hungarian Architects and Engineers, October, pp. 355-358.

Mayne, P.W., and Kulhawy, F.H. (1982). "Ko-OCR Relationships in Soil", Journal of the Geotechnical Engineering Division, ASCE, Vol. 108, No. GT6, pp. 851-872.

Rankine, W.J.M. (1857). "On the Stability of Loose Earth", Philosophical Transactions of the Royal Society, Vol. 147, London.

See Also

stressHorizontal

Examples

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##  Example code for Coefficient of lateral earth pressure
K(sigmax = 50, sigmaz = 90)

##  Example code for Coefficient of lateral earth pressure at rest
Ko(phi = 20, OCR = 1)

##  Example code for Coefficient of lateral earth pressure (active)
Ka(phi = 30, beta = 10)

##  Example code for Coefficient of lateral earth pressure (passive)
Kp(phi = 30, beta = 10)

geotech documentation built on May 1, 2019, 9:09 p.m.